| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8911405 | Journal of Volcanology and Geothermal Research | 2018 | 26 Pages |
Abstract
The seismicity belonging to G1 is located between the deep and intermediate magma storages of Stromboli and seems to precede the 2007 and 2014 effusive eruptions. This suggests that faulting episodes occur as a response to local stress linked to the pressurization of the magmatic system caused by magma ascent.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Salvatore Gambino, Antonio Scaltrito,